Eggshell of the African Ostrich, Struthio camelus, frequently occurs in African archaeological sites, some of which are beyond the limit of radiocarbon dating. In order to date those sites beyond the range of ¹⁴C dating using amino acid geochemistry, an understanding of the reaction kinetics governing amino acid chemistry must be achieved. The integrity of the eggshell matrix provides an excellent medium to investigate the kinetics of protein hydrolysis, amino acid decomposition, and isoleucine epimerization. Mathematical equations are derived from high temperature simulations of time and well-dated sites at ambient temperatures to determine rate constants for the reactions to a D/L ratio of 1.0. The reactions studied are Free and Total isoleucine epimerization, "classical" and "extended" hydrolysis, and the change in concentrations of free, bound, and total amino acids. Arrhenius plots aided in deriving the equations for each method which are then applied to predict kinetic parameters. Temperatures can be predicted within a 2°C range and time within 15% of its actual value if the appropriate method is used.

Thesis (Ph. D.)--University of Wisconsin--Madison, 1967. / Typescript. Vita. Description based on print version record. Includes bibliographical references (leaves [178]-181).

No description available.

A resolução temporal é uma questão-chave em Paleontologia, uma vez que a sua magnitude define a precisão dos estudos não somente paleoecológicos como também evolutivos. A resolução temporal é estimada pela magnitude de time-averaging (mistura de gerações em uma camada, uma amostra). Tais estimativas têm sido amplamente conduzidas em ambientes marinhos recentes. A plataforma continental do sul do Brasil (PSB; 22°S – 34°S) tem sido um laboratório natural para estudos desta natureza desde o início do século XXI. Consequentemente, possui um amplo acervo de dados disponíveis para comparação. Neste contexto, esta tese visou responder (i) qual a magnitude do time-averaging em acumulações de bivalves da PSB? (ii) como este processo varia ao longo de gradientes espaciais? e (iii) como o time-averaging reflete na informação biológica preservada no registro fóssil? Para isto, mais de 140 espécimes de bivalves foram datados integrando racemização de aminoácidos e 14C AMS. Além disto, análises tafonômicas foram realizadas em todas as amostras datadas, incluindo mais sete amostras em sedimentos lamosos. A resolução temporal (time-averaging) e a variabilidade total de idades (mistura temporal) basearam-se em uma nova abordagem numérica, a estatística bayesiana, que integra os erros e as incertezas derivadas da distribuição posterior dos resíduos associados com os modelos resultantes das calibrações das idades. As tendências onshore-offshore — aumento da mediana e da uniformidade das curvas de frequência de distribuição de idades, redução da variabilidade tafonômica, ainda que a escala do time-averaging seja invariante — provavelmente refletem a interação entre as mudanças do nível relativo do mar e da bioprodutividade mais elevada em águas menos profundas. / The temporal resolution of the fossil record plays a key role in paleontology because it determines the scale and the precision of paleoecological and evolutionary studies. The temporal resolution of the fossil record is estimated by the magnitude of time-averaging (non-contemporaneous generations preserved in a single layer, a bulk-sample). Quantitative estimates of time-averaging have been conducted primarily on mollusk shells from modern shallow-water marine settings. Most of them have been addressed in the Southern Brazilian continental shelf (SBS; 22°S up to 34°S), which is considered a natural laboratory for several similar studies since the earlier of current century (XXI). Consequently, the SBS has several available datasets that allow comparisons of the new results displayed here with those previous data. Thus, this thesis aimed answer (i) what is the magnitude of time-averaging on SBS mollusk death assemblages? (ii) how does time-averaging vary across spatial gradients? and (iii) how does time-averaging can reflect on the preservation of the fossil record? Here, >140 specimens were individually dated using amino acid racemization calibrated using radiocarbon ages (14C). In addition, taphonomic analyses were conducted in all samples, including more seven muddy sites. The time-averaging and the total age variability was based on a Bayesian approach that integrates the estimation errors and uncertainties derived from the posterior distribution associated with the 14C–AAR calibration average model. The onshore-offshore trends — increased median age, decreased skewness of age distributions, decreased taphonomic variation, yet the invariant scale of time-averaging — likely reflect the interplay between sea-level changes and elevated bioproductivity in shallower water settings.

A resolução temporal é uma questão-chave em Paleontologia, uma vez que a sua magnitude define a precisão dos estudos não somente paleoecológicos como também evolutivos. A resolução temporal é estimada pela magnitude de time-averaging (mistura de gerações em uma camada, uma amostra). Tais estimativas têm sido amplamente conduzidas em ambientes marinhos recentes. A plataforma continental do sul do Brasil (PSB; 22°S – 34°S) tem sido um laboratório natural para estudos desta natureza desde o início do século XXI. Consequentemente, possui um amplo acervo de dados disponíveis para comparação. Neste contexto, esta tese visou responder (i) qual a magnitude do time-averaging em acumulações de bivalves da PSB? (ii) como este processo varia ao longo de gradientes espaciais? e (iii) como o time-averaging reflete na informação biológica preservada no registro fóssil? Para isto, mais de 140 espécimes de bivalves foram datados integrando racemização de aminoácidos e 14C AMS. Além disto, análises tafonômicas foram realizadas em todas as amostras datadas, incluindo mais sete amostras em sedimentos lamosos. A resolução temporal (time-averaging) e a variabilidade total de idades (mistura temporal) basearam-se em uma nova abordagem numérica, a estatística bayesiana, que integra os erros e as incertezas derivadas da distribuição posterior dos resíduos associados com os modelos resultantes das calibrações das idades. As tendências onshore-offshore — aumento da mediana e da uniformidade das curvas de frequência de distribuição de idades, redução da variabilidade tafonômica, ainda que a escala do time-averaging seja invariante — provavelmente refletem a interação entre as mudanças do nível relativo do mar e da bioprodutividade mais elevada em águas menos profundas. / The temporal resolution of the fossil record plays a key role in paleontology because it determines the scale and the precision of paleoecological and evolutionary studies. The temporal resolution of the fossil record is estimated by the magnitude of time-averaging (non-contemporaneous generations preserved in a single layer, a bulk-sample). Quantitative estimates of time-averaging have been conducted primarily on mollusk shells from modern shallow-water marine settings. Most of them have been addressed in the Southern Brazilian continental shelf (SBS; 22°S up to 34°S), which is considered a natural laboratory for several similar studies since the earlier of current century (XXI). Consequently, the SBS has several available datasets that allow comparisons of the new results displayed here with those previous data. Thus, this thesis aimed answer (i) what is the magnitude of time-averaging on SBS mollusk death assemblages? (ii) how does time-averaging vary across spatial gradients? and (iii) how does time-averaging can reflect on the preservation of the fossil record? Here, >140 specimens were individually dated using amino acid racemization calibrated using radiocarbon ages (14C). In addition, taphonomic analyses were conducted in all samples, including more seven muddy sites. The time-averaging and the total age variability was based on a Bayesian approach that integrates the estimation errors and uncertainties derived from the posterior distribution associated with the 14C–AAR calibration average model. The onshore-offshore trends — increased median age, decreased skewness of age distributions, decreased taphonomic variation, yet the invariant scale of time-averaging — likely reflect the interplay between sea-level changes and elevated bioproductivity in shallower water settings.

A resolução temporal é uma questão-chave em Paleontologia, uma vez que a sua magnitude define a precisão dos estudos não somente paleoecológicos como também evolutivos. A resolução temporal é estimada pela magnitude de time-averaging (mistura de gerações em uma camada, uma amostra). Tais estimativas têm sido amplamente conduzidas em ambientes marinhos recentes. A plataforma continental do sul do Brasil (PSB; 22°S – 34°S) tem sido um laboratório natural para estudos desta natureza desde o início do século XXI. Consequentemente, possui um amplo acervo de dados disponíveis para comparação. Neste contexto, esta tese visou responder (i) qual a magnitude do time-averaging em acumulações de bivalves da PSB? (ii) como este processo varia ao longo de gradientes espaciais? e (iii) como o time-averaging reflete na informação biológica preservada no registro fóssil? Para isto, mais de 140 espécimes de bivalves foram datados integrando racemização de aminoácidos e 14C AMS. Além disto, análises tafonômicas foram realizadas em todas as amostras datadas, incluindo mais sete amostras em sedimentos lamosos. A resolução temporal (time-averaging) e a variabilidade total de idades (mistura temporal) basearam-se em uma nova abordagem numérica, a estatística bayesiana, que integra os erros e as incertezas derivadas da distribuição posterior dos resíduos associados com os modelos resultantes das calibrações das idades. As tendências onshore-offshore — aumento da mediana e da uniformidade das curvas de frequência de distribuição de idades, redução da variabilidade tafonômica, ainda que a escala do time-averaging seja invariante — provavelmente refletem a interação entre as mudanças do nível relativo do mar e da bioprodutividade mais elevada em águas menos profundas. / The temporal resolution of the fossil record plays a key role in paleontology because it determines the scale and the precision of paleoecological and evolutionary studies. The temporal resolution of the fossil record is estimated by the magnitude of time-averaging (non-contemporaneous generations preserved in a single layer, a bulk-sample). Quantitative estimates of time-averaging have been conducted primarily on mollusk shells from modern shallow-water marine settings. Most of them have been addressed in the Southern Brazilian continental shelf (SBS; 22°S up to 34°S), which is considered a natural laboratory for several similar studies since the earlier of current century (XXI). Consequently, the SBS has several available datasets that allow comparisons of the new results displayed here with those previous data. Thus, this thesis aimed answer (i) what is the magnitude of time-averaging on SBS mollusk death assemblages? (ii) how does time-averaging vary across spatial gradients? and (iii) how does time-averaging can reflect on the preservation of the fossil record? Here, >140 specimens were individually dated using amino acid racemization calibrated using radiocarbon ages (14C). In addition, taphonomic analyses were conducted in all samples, including more seven muddy sites. The time-averaging and the total age variability was based on a Bayesian approach that integrates the estimation errors and uncertainties derived from the posterior distribution associated with the 14C–AAR calibration average model. The onshore-offshore trends — increased median age, decreased skewness of age distributions, decreased taphonomic variation, yet the invariant scale of time-averaging — likely reflect the interplay between sea-level changes and elevated bioproductivity in shallower water settings.

Orientador: Jose Augusto Rosario Rodrigues / Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Quimica / Made available in DSpace on 2018-08-06T22:10:42Z (GMT). No. of bitstreams: 1 Cazetta_Tarcila_M.pdf: 2659471 bytes, checksum: 6442c1413f9265995259e16534d2f3cd (MD5) Previous issue date: 2006 / Mestrado / Quimica Organica / Mestre em Química

No description available.

京都大学 / 新制・課程博士 / 博士(工学) / 甲第24640号 / 工博第5146号 / 新制||工||1983(附属図書館) / 京都大学大学院工学研究科合成・生物化学専攻 / (主査)教授 杉野目 道紀, 教授 生越 友樹, 教授 松田 建児 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DGAM

It is important to evaluate periodic fluctuations in environment or climate recorded through time to better understand the nature of Earth's history as well as to develop ideas about what the future may hold. There exist numerous proxies by which these environmental patterns can be demonstrated and analyzed through various time scales; from sequence stratigraphic bundles of transgressive-regressive cycles that demonstrate eustatic changes in global sea level, to the geochemical composition of a skeleton that records fluctuations in ocean temperature through the life of the biomineralizing organism. This study examines some of the methods by which we can analyze environmental fluctuations recorded at different time scales. The first project examines the methods by which extrabasinal orbital forcing (i.e. Milankovitch cycles) can be tested in the rock record. In order to distinguish these patterns, computer generated carbonate rock records were simulated with the resulting outcrops tested using common methods. These simulations were built upon eustatic sea level fluctuations with periods similar to what has been demonstrated in the rock record, as well as maintaining the many factors that affect the resultant rock composition such as tectonics, subsidence, and erosion. The result demonstrated that substantially large sea level fluctuations, such as those that occur when the planet is in an icehouse condition, are necessary to produce recognizable and preservable patterns that are otherwise overwhelmed by other depositional factors. The second project examines the temporal distribution of the bivalve Semele casali from Ubatuba Bay, Brazil by using amino acid racemization (AAR) calibrated with ¹⁴C radiometric dates. This data set is one of the largest ever compiled and demonstrates that surficial shell assemblages in the area have very long residence times extending back in time 10,000 years. The area has had very little change in sea level and the AAR ratios which are highly temperature dependent could be calibrated across sites varying from 10 to 53 meters in water depth. Long time scales of dated shells provide us with an opportunity to study climate fluctuations such as El Niño southern oscillation. The third project describes a newly developed method for estimating growth rates in organisms using closely related species from similar environments statistically analyzed for error using a jackknife corrected parametric bootstrap. As geochemical analyses get more precise while using less material, data can be collected through the skeleton of a biomineralizing organism, thus revealing information about environmental shifts at scales shorter than a year. For such studies, the rate of growth of an organism has substantial effects on the interpretation of results, and such rates of growth are difficult to ascertain, particularly in fossilized specimens. This method removes the need for direct measures of growth rates and even the most conservative estimates of growth rates are useful in constraining the age ranges of geochemical intra-skeletal studies, thus elucidating the likely time period under analysis. This study assesses the methods by which periodic environmental fluctuations at greatly varying time scales can be used to evaluate our understanding of earth processes using rigorous quantitative strategies. / Ph. D.